Open Access40Ar/39Ar age of the gold-silver Burinda deposit and its relationship to magmatism (north-eastern part of the argun superterrane)
Author(s) -
И. В. Бучко,
И. В. Бучко,
А. А. Сорокин,
А. А. Сорокин,
В. А. Пономарчук,
В. А. Пономарчук,
А. В. Травин,
А. В. Травин
Publication year - 2019
Publication title -
doklady akademii nauk. rossijskaâ akademiâ nauk
Language(s) - English
Resource type - Journals
ISSN - 0869-5652
DOI - 10.31857/s0869-56524853321-325
Subject(s) - magmatism , hydrothermal circulation , geology , geochemistry , volcano , mineralogy , paleontology , tectonics
It was established that the age of hydrothermal ore metasomatites of the Burinda gold-silver deposit, one of the most famous in eastern Asia, can be estimated in the interval 126-128 Ma. It is shown that the formation of this deposit is due to hydrothermal processes in the final stages of the formation of the Taldan volcanic complex.